4.3 Mathematical Machinery 227
simply amounts to the requirement that each α
(t), regarded as a vector in
M
5
is spacelike, timelike or null in M
5
. We will say that a timelike or null
curve in dS is future-directed (resp., past-directed )ifeachα
(t), regarded as
a vector in M
5
, is future-directed (resp., past-directed).
Remark: The notion of a spacetime, as we have defined it, is very general
and there are examples in which it is not possible to define unambiguous
notions of future-directed and past-directed (see [HE], page 130). This is
essentially a sort of “orientability” issue analogous to the fact that, for some
surfaces in R
3
such as the M¨obius strip, it is impossible to define a continuous
nonzero normal vector field over the entire surface. We care only about M
and dS and so the issue will not arise for us.
A future-directed timelike curve in dS is called a timelike worldline and we
ascribe to such a curve the same physical interpretation we did in M (the
worldline of some material particle). Just as in M one can define the proper
time length L(α)ofsuchacurveα :[a, b] → dS by
L(α)=
b
a
−(α
(t),α
(t)) dt
and a proper time parameter τ = τ(t)alongα by
τ = τ(t)=
t
a
−(α
(u),α
(u)) du.
We will go even further and induce causality relations on dS from those on
M
5
. Specifically, for distinct points x and y in dS we will define x y if and
only if y − x is timelike and future-directed in M
5
and x<yif and only if
y − x is null and future-directed in M
5
.
Remark: Although we will have no need of the result, we point out that,
with these definitions, Zeeman’s Theorem 1.6.2 remains true in dS in the
following sense. A bijection F : dS → dS that preserves < in both directions
also preserves in both directions and is, in fact, the restriction to dS of
some orthochronous orthogonal transformation of M
5
(see [Lest]).
Let us think for a moment about the sort of timelike curve in dS that
should model the worldline of a material particle that is “free”, i.e., in free
fall. As we saw in Section 4.2, at each point on such a worldline there is a
local inertial frame (freely falling elevator) from which it can be observed
and that, relative to such a frame, the worldline will appear (approximately)
“straight.” Curves in a manifold with (Riemannian or Lorentz) metric that
are “locally straight” are called geodesics. There are various approaches to the
formulation of a precise definition, but we will follow a path that is adapted
to the simplicity of the examples we wish to consider. The motivation for our
approach is most easily understood in the context of smooth surfaces in R
3
so we will first let the reader work through some of this.